General Information
Secondary Commodities: coal
Deposit Type(s): Coal
Location(s): 60.030830 N, -128.763330 W
NTS Mapsheet(s): 105A02
Location Comments: .5 Kilometres
Hand Samples Available at YGS: No
Capsule
Work History
This coal occurrence was first noted in 1887 by G.M. Dawson and first staked as Carol cl (Y27509) in May/68 by C. Sporer. Canex Placer acquired this occurrence as Coal Exploration Licence #61 in Oct/76, and as Licence #113 in Oct/79 and bulldozer trenched and drilled one hole (187 m) in 1977.
In Aug/94 Cash Resources Ltd acquired by application Coal Exploration Licences Y - 460 - 464 and in 1995 dug 3 trenches (TR - 12-14) near the occurrence.
Capsule Geology
Upper Paleocene or Lower Eocene coal of lignite A and B ranks is exposed in a trench. A 1.5 m thick seam underlain by grey claystone has an observed dip of 35°N. The sediments in the Watson Lake basin exhibit upward fining and thinning and are interpreted as point bar sequences produced by meandering streams.
Permafrost was encountered in all three trenches and no coal seams were encountered.
This coal occurrence was first noted in 1887 by G.M. Dawson and first staked as Carol cl (Y27509) in May/68 by C. Sporer. Canex Placer acquired this occurrence as Coal Exploration Licence #61 in Oct/76, and as Licence #113 in Oct/79 and bulldozer trenched and drilled one hole (187 m) in 1977.
In Aug/94 Cash Resources Ltd acquired by application Coal Exploration Licences Y - 460 - 464 and in 1995 dug 3 trenches (TR - 12-14) near the occurrence.
Capsule Geology
Upper Paleocene or Lower Eocene coal of lignite A and B ranks is exposed in a trench. A 1.5 m thick seam underlain by grey claystone has an observed dip of 35°N. The sediments in the Watson Lake basin exhibit upward fining and thinning and are interpreted as point bar sequences produced by meandering streams.
Permafrost was encountered in all three trenches and no coal seams were encountered.
Location Map
Last Updated: May 28, 2014
Work History
Year | Work Type | Comment |
---|---|---|
1995 | Trenching: Mechanical | Permafrost was encountered in all 3 trenches and no coal seams were encountered. |
1977 | Drilling: Diamond | Number of holes drilled: 1 Amount of work done: 187 m |
1977 | Trenching | |
1887 | Other | First noted by G. M. Dawson of Geological Survey of Canada. |
Regional Geology - Terrane
Group: Ancestral North America
Affinity: W Laurentia
Name: Cassiar
Realm: Laurentia
Regional Geology - Bedrock
Supergroup:
Group/Suite: Ross?
Formation:
Member:
Terrane:
Period Max: Paleogene
Age Max: 58 MA
Period Min: Paleogene
Age Min: 48 MA
Rock Major: conglomerate, shale, coal
Rock Minor:
Reference: Mortensen & Murphy (2005) - YGS OF 2005-10
Geological Unit (1M): lTR
Geological Unit (250K): lTR3
Related References
Number | Title | Page(s) | Document Type |
---|---|---|---|
ARMC007827 | Heavy mineral sampling map - Watson Lake - Anmac project | Geochemical Map | |
MIR1978 | Mineral Industry Report 1978 | 73 | Annual Report |
YCI1994 | Yukon Coal Inventory | Report |
Citations |
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Dawson, G.M., 1889. Report on an exploration in the Yukon District, NWT, and adjacent northern portion of British Columbia, 1887. In: Geological and Natural History Survey of Canada reports and maps of investigations and surveys, 1887-1888, Selwyn, A.R.C. (ed.). Geological Survey of Canada, Annual Report vol. 3, (1887-1888), p. 101B. |
Hughes, J.D. and Long, D.G.F., 1980. Geology and coal resource potential of Early Tertiary strata along Tintina Trench, Yukon Territory. Geological Survey of Canada, Paper 79-32, 21 p. |
Lord, C.S., 1944. Geological reconnaissance along the Alaska Hwy between Watson Lake and Teslin River, Yukon and British Columbia. Geological Survey of Canada, Paper 44-25, p. 19. |